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http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79806完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 胡植慶(Jyr-Ching Hu) | |
| dc.contributor.author | Ting-Yun Lee | en |
| dc.contributor.author | 李庭昀 | zh_TW |
| dc.date.accessioned | 2022-11-23T09:12:03Z | - |
| dc.date.available | 2021-08-11 | |
| dc.date.available | 2022-11-23T09:12:03Z | - |
| dc.date.copyright | 2021-08-11 | |
| dc.date.issued | 2021 | |
| dc.date.submitted | 2021-08-09 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79806 | - |
| dc.description.abstract | 札格羅斯造山帶是阿爾卑斯－喜馬拉雅造山系統的一部分，由阿拉伯板塊及歐亞板塊間的陸－陸碰撞所生成。造山帶前方的前陸盆地是世界上重要的產油區之一，位於造山帶西北方的基爾庫克弧凹所含之油氣儲藏量約佔盆地總儲量的18 %，但其油氣探勘程度相較於中東其他國家較低，故若能對此區域的構造演化模式有更完整的了解，應有助於增加油氣探勘的準確性。本研究可分為兩個部分，第一部分利用MOVE軟體回復前人所發表的構造平衡剖面，探討長期構造演化歷史，結果顯示此處的構造大致遵循由東北向西南傳遞的順時序（in-sequence）演化，且基盤逆衝斷層多未穿出沈積層出露至地表，而是向上連結至區域的基底滑脫層。剖面在回復後共產生了約16.3公里的縮短量，縮短率約7 %，不同構造區的地層縮短量大致由後陸向前陸方向遞減，此外後陸之基盤斷層所產生的水平壓縮量與沈積層中因滑脫褶皺作用所產生的地層縮短量非常接近，然而前陸之基盤斷層所產生的水平壓縮量卻未完全反映於此處的沈積層之中，此現象反映了縮短量會沿滑脫層向前陸傳遞的情形。在研究的第二部分，利用小基線子集法（Small Baseline Subset）處理D-InSAR之資料，對研究區域內主要的構造進行地表變形觀測，此部分的結果顯示山前斷層及基爾庫克斷層周圍有明顯的地表變形特徵，其上盤地表分別以約10 mm/yr及20 mm/yr的速率抬升，代表此二構造屬於基爾庫克地區近年來具有較高活動性的構造。最後綜合兩部分的研究結果，與地震活動分布進行比較，可歸納出此處由東北向西南擴展的活躍造山運動，使源自脆－塑性轉換帶的基盤斷層大致以順時序的模式參與變形，這些基盤斷層向上連結至基底滑脫層，使縮短量沿著滑脫層向前陸傳遞，使沈積層產生滑脫褶皺。而基盤的構造活動所產生之地層縮短量尚未完全反映至前陸的變形之中，然而前陸現今的構造活動性有提升的趨勢，說明了地層的水平縮短仍然在持續，且較大的變形應會沿軟弱岩層發生。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2022-11-23T09:12:03Z (GMT). No. of bitstreams: 1 U0001-0808202100101900.pdf: 85332228 bytes, checksum: fa9db71901058052d9fa6d08ad78c2cb (MD5) Previous issue date: 2021 | en |
| dc.description.tableofcontents | 口試委員會審定書 I 致謝 II 摘要 III Abstract III 目錄 VI 圖目錄 IX 表目錄 XIII 第一章 緒論 1 1.1 前言 1 1.2 前人研究 4 1.2.1 造山帶變形模式 4 1.2.2 札格羅斯造山帶構造特徵 8 1.2.3 地表及地下地質調查 11 1.2.4 區域地質構造剖面 15 1.2.5 InSAR於地表變形觀測之應用 20 第二章 地體構造與地質背景 24 2.1 造山帶演化歷史 24 2.1.1 新元古代－晚泥盆紀：被動大陸邊緣階段 24 2.1.2 晚泥盆紀－晚二疊紀：主動大陸邊緣階段 24 2.1.3 晚二疊紀－晚白堊紀：新特提斯洋的發育與被動大陸邊緣階段 25 2.2.4 晚白堊紀至今：札格羅斯造山運動 25 2.2 構造區劃 29 2.3 研究區域 32 2.3.1 地層概況 32 2.3.2 構造概況 42 2.4 活動構造 48 2.4.1 GPS速度場及應變速率 48 2.4.2 地震活動特性 51 第三章 研究資料與方法 55 3.1 地質構造平衡剖面 55 3.1.1 地質構造剖面建構理論及方法 55 3.1.2 構造平衡剖面之回復 57 3.2 地震資料 61 3.3 地表變形時間序列分析 61 3.3.1 合成孔徑雷達干涉技術（InSAR） 61 3.3.2 小基線子集法（Small Baseline Subset） 64 3.3.3 InSAR時間序列處理 64 第四章 研究成果 71 4.1 地質剖面解釋 71 4.1.1 剖面A段－低褶皺帶 72 4.1.2 剖面B段－外部高褶皺帶 73 4.1.3 剖面C段－內部高褶皺帶 73 4.1.4 剖面構造演化時序 78 4.2 構造平衡剖面之回復 80 4.2.1 低褶皺帶變形之回復（Step 1） 80 4.2.2 山前斷層之回復（Step 2） 80 4.2.3 外部高褶皺帶變形之回復（Step 3） 81 4.2.4 馬庫克背斜下方基盤逆衝斷層之回復（Step 4） 81 4.2.5 內部高褶皺帶變形之回復（Step 5） 82 4.3 InSAR地表變形時間序列 91 4.3.1 InSAR累積位移量 93 4.3.2 InSAR平均位移速率 103 4.3.3 InSAR 2.5D平均位移速率 106 第五章 討論 109 5.1 構造縮短量與擠壓速度 109 5.2 斷層滑移量與地層縮短量 113 5.3 地震活動分佈 115 5.4 低褶皺帶之構造活動特性 118 5.5 2017年Mw 7.3兩伊邊境地震之震後變形趨勢 120 第六章 結論 123 參考文獻 125 附錄一：雷達影像編號與對應日期 132 附錄二：雷達影像干涉對與對應之垂直基線長 134 | |
| dc.language.iso | zh-TW | |
| dc.subject | 小基線子集法 | zh_TW |
| dc.subject | 札格羅斯造山帶 | zh_TW |
| dc.subject | 基爾庫克弧凹 | zh_TW |
| dc.subject | InSAR | zh_TW |
| dc.subject | 平衡剖面 | zh_TW |
| dc.subject | InSAR | en |
| dc.subject | Small Baseline Subset | en |
| dc.subject | Balanced cross section | en |
| dc.subject | Zagros orogen | en |
| dc.subject | Kirkuk recess | en |
| dc.title | 札格羅斯造山帶基爾庫克弧凹之構造演化及活動性 | zh_TW |
| dc.title | Structural Evolution and Activity of Kirkuk Recess in Zagros Orogen | en |
| dc.date.schoolyear | 109-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 黃鐘(Hsin-Tsai Liu),謝嘉聲(Chih-Yang Tseng),賴光胤,蔡旻倩 | |
| dc.subject.keyword | 平衡剖面,札格羅斯造山帶,基爾庫克弧凹,InSAR,小基線子集法, | zh_TW |
| dc.subject.keyword | Balanced cross section,Zagros orogen,Kirkuk recess,InSAR,Small Baseline Subset, | en |
| dc.relation.page | 139 | |
| dc.identifier.doi | 10.6342/NTU202102180 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2021-08-10 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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